Monitoring water floods using potentials between casing-mounted electrodes
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[0026]Disclosed herein are various techniques for monitoring the locations of water floods adjacent to a well. A water flood approaching a well causes resistivity changes in the formation surrounding the well. The significance of these formation resistivity changes increases with greater proximity to the water flood. Accordingly, the techniques disclosed herein include injecting current into the formation surrounding the well and measuring potentials between a well casing and electrodes mounted circumferentially about the casing, or between the electrodes themselves. Although the current is injected (e.g., via the casing) in an azimuthally uniform manner, the potentials measured at the different electrodes will vary depending on their respective proximities to the water flood. Because these electrode potentials directly reflect water flood proximity, they can be measured and analyzed to determine the locations of the water floods.
[0027]FIGS. 1-3 represent various subterranean enviro...
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